User:Ajdu93/sandbox

Process

 * petrification is the process in which organic matter is converted to stone through the replacement of the original material and the filling of pore spaces materials
 * takes place through combination of two similar processes-permineralization, and replacement

Permineralization

 * permineralized fossiles still contain fair amount of original material
 * occurs when groundwater containing dissolved minerals fills pore spaces and cavities of specimens, particularly bone, shell or wood
 * pores of organism are filled with minerals that precipitate out of water
 * common type of permineralization is silicification

Silicification

 * process in which organic matter becomes saturated with silica
 * most of organic matter is destroyed
 * volcanic material is often source of silica for silicification
 * usually occurs in two environments
 * either specimens get buried in sediments of deltas and floodplains or organisms get buried in volcanic ash
 * must have water present because it reduces oxygen and therefore reduces deterioration by fungi, maintains wood shape, allows for transportation and deposition of silica
 * process begins when wood or organism is permeated with silica solution
 * cell walls progressively dissolved, silica is deposited in any empty spaces
 * organism is transformed to stone (process called lithification) as water is lost
 * as the process proceeds, cellulose and lignin degrade and are replaced
 * can occur in 50,000 years or less under geothermal conditions

Replacement

 * occurs when water containing dissolved minerals dissolves original solid material of organism, which are replaced by minerals
 * can take place extremely slowly and can replicate original microscopic structure or organism
 * minerals commonly used in replacement are calcite, silica, pyrite and hematite
 * rare, but very important to paleontologists because these fossils are very detailed

Uses

 * primarily used as museum exhibits
 * used in fine art
 * also used in furniture as table tops

=Petrification= In geology, petrification is the process in which organic matter is converted to stone through the replacement of the original material and the filling of pore spaces of the original material. Petrification takes place through combination of two similar processes-permineralization and replacement. The best known result of this process is petrified wood, but all organisms, from bacteria to vertebrates, can be petrified.

Permineralization
One of the processes involved in petrification is permineralization. The fossils created through this process tend to contain a large amount of the original material of the specimen. This process occurs when groundwater containing dissolved minerals (most commonly quartz, calcite, pyrite, siderite (iron carbonate), apatite (calcium phosphate) ), fills pore spaces and cavities of specimens, particularly bone, shell or wood. The pores of the organisms' tissues are filled when these minerals precipitate out of the water. Two common types of permineralization are silicification and pyritization.

Silicification
Silicification is the process in which organic matter becomes saturated with silica. A common source of silica is volcanic material. Studies done by Sigleo and Mustoe have shown that in this process, most of the original organic matter is destroyed. Silicification most often occurs in two environments-either the specimen is buried in sediments of deltas and floodplains or organisms are buried in volcanic ash. Water must be present for silicification to occur because it reduces the amount of oxygen present and therefore reduces the deterioration of the organism by fungi, maintains organism shape, and allows for the transportation and deposition of silica. The process begins when a specimen is permeated with an aqueous silica solution. The cell walls of the specimen are progressively dissolved and silica is deposited into the empty spaces. In wood samples, as the process proceeds, cellulose and lignin, two components of wood, are degraded and replaced with silica. The specimen is transformed to stone (a process called lithification) as water is lost. For silicification to occur, the geothermic conditions must include a neutral to slightly acidic pH and a temperature and pressure similar to shallow-depth sedimentary environments; under these conditions, silicification can occur in 50,000 years or less.

Pyritization
Pyritization is a process similar to silicification, but instead involves the deposition of iron and sulfur in the pores and cavities of an organism. Pyritization can result in both solid fossils as well as preserved soft tissues. In marine environments, pyritization occurs when organisms are buried in sediments containing a high concentration of iron sulfides. Organisms release sulfide, which reacts with dissolved iron in the surrounding water, when they decay. This reaction between iron and sulfides forms pyrite (FeS2). Carbonate shell material of the organism is then replaced with pyrite due to a higher concentration of pyrite and a lower concentration of carbonate in the surrounding water. Pyritization occurs to a lesser extent in plants in clay environments.

Replacement
Replacement, the second process involved in petrification, occurs when water containing dissolved minerals dissolves the original solid material of an organism, which is then replaced by minerals. This can take place extremely slowly, replicating the microscopic structure of the organism. The slower the rate of the process, the better defined the microscopic structure will be. The minerals commonly involved in replacement are calcite, silica, pyrite, and hematite. It is rare to find organisms preserved by replacement alone (as opposed to in combination with permineralization), but these fossils present significant importance to paleontologists because these fossils tend to be very detailed.

Uses
Not only are the fossils produced through the process of petrification used for paleontological study, but they have also been used as both decorative and informative pieces. Petrified wood is used in several ways. Slabs of petrified would can be crafted into tabletops, or the slabs themselves are sometimes displayed in a decorative fashion. Also, larger pieces of the wood have been carved into sinks and basins. Other large pieces can also be crafted into chairs and stools. Petrified wood and other petrified organisms have also been used in jewelry, sculpture, clock-making, ashtrays and fruit bowls, and landscape and garden decorations.

Petrified Wood in Architecture
Petrified wood has also been used in construction. The Petrified Wood Gas Station, located in Lamar, Colorado, was built in 1932 and consists of walls and floors constructed from pieces of petrified wood over 175 million years old. The structure, built by W.G. Brown, has since been converted to office space and a used car dealership. Glen Rose, Texas provides even more examples of the use of fossilized wood in architecture. Beginning in the 1920s, the farmers of Somervell County, Texas began uncovering 115 million year old petrified trees. Local craftsmen and masons then built over 65 structures from this petrified wood, 45 of which were still standing as of June 2009. These structures include gas stations, flowerbeds, cottages, restaurants, fountains and gateposts. Glen Rose, Texas is also been noted for Dinosaur Valley State Park and the Glen Rose Formation, where fossilized dinosaur footprints from the Cretaceous period, dating back about 110 million years, can be viewed. Another example of the use of petrified wood in construction is the Agate House Pueblo in the Petrified Forest National Park in Arizona. Built by ancestral Pueblo people about 900 years ago, this eight-room building was constructed almost entirely out of petrified wood and is believed to have served as either a family home or ceremonial center.

Artificial Petrification
Scientists have been attempting to artificially petrify organisms as early as the 18th century, when Girolamo Segato succeeded in artificially petrifying human remains. His methods were lost, but the bulk of his "pieces" are on display at the Museum of the Department of Anatomy in Florence, Italy. More recent attempts have been both successful and documented. Hamilton Hicks of Greenwich, Connecticut, patented his "recipe" for rapid artificial petrification of wood in1986. Hicks' recipe consists of highly mineralized water and a sodium silicate solution combined with a dilute acid with a pH of 4.0-5.5. Samples of wood are then penetrated with this mineral solution through repeated submersions and applications of the solution. Wood treated in this fashion is incapable of being burned and acquires the features of petrified wood. Some uses of this product as suggested by Hicks include use by horse breeders who desire fireproof stables constructed of nontoxic material that would also be resistant to chewing of the wood by horses.

This is some sample text from my annotated bibliography.

This source provides another view and description of the basic types of organism preservation. It also provides insight into several different types of fossils and how they form. I will use this source to compare and contrast these different forms of fossilization with my primary topic, petrification.